1887

Abstract

In the Neuquén province of Argentina (37° - 40° S), several Andean intermontane basins contain Oligocene<br>to Miocene continental strata. Despite claims that these basins developed as rifts (Jordan et al., 2001; Burns et<br>al., in press), we have good evidence that two basins developed in a compressional setting.

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/content/papers/10.3997/2214-4609-pdb.111.79
2006-09-24
2021-12-08
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